How SeismoAlert Works?
TSW Window: 1838-06-18T02:33:07Z to 1838-06-26T02:33:07Z
Syzygy Time: 1838-06-22T02:33:07Z
Perigee Time: N/A
Sublunar Latitude: 28.407735127°
Sublunar Longitude: 141.9357398772°
TSB Lower Latitude: 13.4077°
TSB Upper Latitude: 43.4077°
Syzygy: 6.7378038298 kPa
Perigee: 0 kPa
Syzygy: 4.0426822979 kPa
Perigee: 0 kPa
Philippine Plate / Mexico / Caribbean/ Red Sea Rift, San Andreas / Himalayan / Mediterranean, Kuril-Kamchatka / Cascadia / N. Japan
Perigee In Tsw: No
Perihelion In Tsw: No
Mars In Tsw: Yes
Venus In Tsw: Yes
Super Tsw: Yes
The June 1838 San Andreas earthquake is estimated to have had a magnitude of M 6.8 to 7.5. It ruptured the Santa Cruz Mountains and Peninsula sections of the San Andreas Fault. Witnesses at the time—largely from the missions and early ranchos—reported severe shaking that lasted for several minutes, causing significant damage from Monterey to San Francisco.
Our computed data focuses on the relationship between lunar/planetary positions and seismic stress. Here is a breakdown of what those metrics represent in this context:
The earthquake actually occurred around June 23, 1838. This fits remarkably well within our TSW Window (June 18–26) and is just one day after our noted Syzygy Time of June 22. This high degree of correlation is exactly what researchers look for when studying tidal triggering theories.
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